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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>4</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2004</publication_year>
	</journal>
	<doi>10.5194/acpd-4-3535-2004</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/4/3535/2004/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/4/3535/2004/acpd-4-3535-2004.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/4/3535/2004/acpd-4-3535-2004.pdf</fulltext_pdf>
	<start_page>3535</start_page>
	<end_page>3563</end_page>
	<publication_date>2004-06-25</publication_date>
	<article_title content_type="html">Atmospheric particle formation events at Värriö measurement station in Finnish Lapland 1998–2002</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>H. Vehkamäki</name>
			<email>hanna.vehkamaki@helsinki.fi</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>M. Dal Maso</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>T. Hussein</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>R. Flanagan</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>A. Hyvärinen</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>J. Lauros</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>J. Merikanto</name>
		</author>
		<author numeration="8" affiliations="1">
			<name>P. Mönkkönen</name>
		</author>
		<author numeration="9" affiliations="1">
			<name>M. Pihlatie</name>
		</author>
		<author numeration="10" affiliations="2">
			<name>K. Salminen</name>
		</author>
		<author numeration="11" affiliations="1">
			<name>L. Sogacheva</name>
		</author>
		<author numeration="12" affiliations="2">
			<name>T. Thum</name>
		</author>
		<author numeration="13" affiliations="1">
			<name>T. Ruuskanen</name>
		</author>
		<author numeration="14" affiliations="1">
			<name>P. Keronen</name>
		</author>
		<author numeration="15" affiliations="1">
			<name>P. P. Aalto</name>
		</author>
		<author numeration="16" affiliations="3">
			<name>P. Hari</name>
		</author>
		<author numeration="17" affiliations="1">
			<name>K. E. J. Lehtinen</name>
		</author>
		<author numeration="18" affiliations="1">
			<name>Ü. Rannik</name>
		</author>
		<author numeration="19" affiliations="1">
			<name>M. Kulmala</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Physical Sciences, P.O. Box 64, University of Helsinki, 00014 Helsinki, Finland</affiliation>
		<affiliation numeration="2" content_type="html">Finnish Meteorological Institute, P.O Box 503, 00101 Helsinki, Finland</affiliation>
		<affiliation numeration="3" content_type="html">Department of Forest Ecology, P.O. Box 27, University of Helsinki, 00014 Helsinki, Finland</affiliation>
	</affiliations>
	<abstract content_type="html">We have identified 147 clear 8 nm diameter particle formation events at the
SMEAR I station in V&amp;#228;rri&amp;#246;, northern Finland during calendar years
1998&amp;ndash;2002. The events have been classified in detail according to the
particle formation rate, growth rate, event starting time, different gas
phase species concentrations and pre-existing particle concentrations as
well as various meteorological conditions. Most of the events occurred
during the spring months between March and May, suggesting that increasing
biological activity might produce the precursor gases for particle
formation. The apparent 8 nm particle formation rates were around 0.1/cm&lt;sup&gt;3&lt;/sup&gt;s,
and they were uncorrelated with growth rates that vary between
0.5 and 10 nm/h. The air masses, which had clearly elevated sulphur dioxide
concentrations above 1.6 ppb came, as expected, from the direction of Nikel
and Monschegorsk smelteries. Only 15 formation events can be explained by
the pollution plume from these sources.</abstract>
	<references>
	</references>
</article>

